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A Closer Look: The Black Guillemots of Cooper Island

This feature tracks the summer water temperature of the Snake River.

  • Line graph showing number of breeding pairs of black guillemot and number of nest sites installed in Cooper Island, Alaska, from 1972 to 2019.
    Download Data   Download Image
     
     

    Reference map showing the location of Utqiagvik, Alaska. This figure shows the number of breeding pairs in the black guillemot colony that inhabit Cooper Island along the north coast of Alaska, measured at the peak of breeding season (green line). The orange line indicates the number of installed nest site structures available to black guillemots on Cooper Island each year.
    Data source: Divoky, 201912
    Web update: April 2021

Line graph showing number of breeding pairs of black guillemot and number of nest sites installed in Cooper Island, Alaska, from 1972 to 2019
Figure 1. Cooper Island Black Guillemot Breeding Pairs, 1972–2019

Key Points | Background | About the Data | Technical Documentation

Key Points

  • The black guillemot population on Cooper Island reached a peak of more than 200 pairs in the late 1980s, but the number has decreased by more than half since then (see Figure 1). In 2019, scientists observed only 85 breeding pairs.
  • Although the initial increase in breeding pairs coincided with an expansion of available nesting sites, the decrease since the 1980s has occurred despite a constant number of nesting sites.
  • The decline over the last three decades has coincided with reduced breeding success,7 earlier egg laying,8 and a decrease in the presence of sea ice in the region,9,10 (see the Arctic Sea Ice indicator).
  • Data from another long-studied colony on the edge of the Beaufort Sea (Herschel Island, Canada) suggest that similar trends are occurring across the western Arctic region.11

Background

A colony of black guillemots have made Cooper Island near Utqiagvik (formerly Barrow), Alaska, home for at least 50 years. The area’s unique landscape and sea ice are integral components of this bird’s habitat. The black guillemot spends the winter on Arctic sea ice, and it breeds on land near the edge of the ice in summer.1 One of the primary food sources for the birds’ chicks is the Arctic cod, which thrives in cold, ice-covered waters. Warming temperatures and other changes are reducing the extent and persistence of Arctic sea ice (see the Arctic Sea Ice indicator), which has been linked to a decline in the abundance of Arctic cod over the last few decades.2

The region has experienced an increase in the number of days without snow cover each year.3 This longer period has helped the black guillemots during breeding season, when they prefer a snow-free nest cavity.4 However, as the Arctic has warmed, sea ice has decreased significantly—melting earlier and freezing later.5 This change, for certain parts of the year, has led to more open water and increased the distance from the coast to the edge of the ice, where these birds forage for Arctic cod.6 This type of ecosystem change has broader implications not only for these two species, but also for other animals in the Arctic that depend on marine prey, such as polar bears, and for people who depend on these animals for food and other resources.

A group of scientists and volunteers have been observing and counting birds at the Cooper Island colony for more than 40 years. Birds are counted every summer and identified as breeding pairs if two are found to be inhabiting a specific nesting site on the island. This long-term record provides valuable clues about how rapid changes being observed in the Arctic may be influencing the natural environment.

About the Data

Notes

Changes in the number of breeding pairs in the Cooper Island colony can be influenced by several factors other than the presence or absence of sea ice and resulting reduced prey availability. These other factors include competition from other bird species, the activity of predators such as polar bears, and the success of and immigration from other black guillemot colonies in the Arctic. The timing and duration of the breeding season can also change in response to changing temperatures and snow and ice conditions. In addition, as the count of breeding pairs depends on the observation of successful egg laying, changes in fertility or nest predation could influence annual totals. Consistent methods have been used to count the number of breeding pairs on Cooper Island annually for more than 40 years.  Guillemots began breeding at Cooper Island sometime after the U.S. Navy left wooden boxes on the island in the mid-1950s, which the birds used for nesting. The colony was officially discovered by researchers in 1972, when it consisted of 10 breeding pairs.13 The researchers began building artificial nest sites, adding 190 sites before they stopped in the mid-1980s. Cooper Island had more breeding pairs than nest sites in the late 1980s, when some of the larger nesting sites were occupied by more than one pair. Additional birds were present but were unable to breed due to the limited number of nest cavities.

Data Sources

The data in this feature are collected by researchers and provided by George Divoky and the Friends of Cooper Island (http://cooperisland.org). This data set has been used and published as part of peer-reviewed journal articles on observed changes in northern Alaska—particularly the region near Utqiagvik.14,15

Technical Documentation

  • Download related technical information PDF

References

1.  Divoky, G.J., D.C. Douglas, and I.J. Stenhouse. 2016. Arctic sea ice a major determinant in Mandt’s black guillemot movement and distribution during wing season. Biol. Lett. 12(9):20160275.http://rsbl.royalsocietypublishing.org/content/12/9/20160275.

2. Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller, M.L. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161. www.sciencedirect.com/science/article/pii/S007966111500107X.

3. Cox, C.J., R.S. Stone, D.C. Douglas, D.M. Stanitski, G.J. Divoky, G.S. Dutton, C. Sweeney, J.C. George, and D.U. Longenecker. 2017. Drivers and environmental responses to the changing annual snow cycle of northern Alaska. Bull. Amer. Meteor. Soc. 98(12):2559–2577. https://journals.ametsoc.org/doi/10.1175/BAMS-D-16-0201.1. doi:10.1175/BAMS-D-16-0201.1.

4. Cox, C.J., R.S. Stone, D.C. Douglas, D.M. Stanitski, G.J. Divoky, G.S. Dutton, C. Sweeney, J.C. George, and D.U. Longenecker. 2017. Drivers and environmental responses to the changing annual snow cycle of northern Alaska. Bull. Amer. Meteor. Soc. 98(12):2559–2577. https://journals.ametsoc.org/doi/10.1175/BAMS-D-16-0201.1. doi:10.1175/BAMS-D-16-0201.1.

5 .USGCRP (U.S. Global Change Research Program). 2017. Climate science special report: Fourth National Climate Assessment, volume I. Wuebbles, D.J., D.W. Fahey, K.A. Hibbard, D.J. Dokken, B.C. Stewart, and T.K. Maycock, eds. https://science2017.globalchange.gov. doi:10.7930/J0J964J6.

6. Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161. www.sciencedirect.com/science/article/pii/S007966111500107X.

7. Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161. www.sciencedirect.com/science/article/pii/S007966111500107X.

8. Cox, C.J., R.S. Stone, D.C. Douglas, D.M. Stanitski, G.J. Divoky, G.S. Dutton, C. Sweeney, J.C. George, and D.U. Longenecker. 2017. Drivers and environmental responses to the changing annual snow cycle of northern Alaska. Bull. Amer. Meteor. Soc. 98(12):2559–2577. https://journals.ametsoc.org/doi/10.1175/BAMS-D-16-0201.1. doi:10.1175/BAMS-D-16-0201.1.

9. USGCRP (U.S. Global Change Research Program). 2017. Climate science special report: Fourth National Climate Assessment, volume I. Wuebbles, D.J., D.W. Fahey, K.A. Hibbard, D.J. Dokken, B.C. Stewart, and T.K. Maycock, eds. https://science2017.globalchange.gov. doi:10.7930/J0J964J6.

10. Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161.

11. Eckert, C.D. 2018. Black guillemot population monitoring at Herschel Island–Qikiqtaruk Territorial Park, Yukon: Outcome of the 2018 nesting season. Yukon Department of Environment.

12. Divoky, J.G. 2019 update to data originally published in: Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161.

13. Divoky, G.J., G.E. Watson, and J.C. Bartonek. 1974. Breeding of the black guillemot in northern Alaska. Condor 76:339–343.

14. Divoky, J.G., M.P. Lukas, and M.L. Druckenmiller. 2015. Effects of recent decreases in arctic sea ice on an ice-associated marine bird. Prog. Oceanogr. 136:151–161.

15. Cox, C.J., R.S. Stone, D.C. Douglas, D.M. Stanitski, G.J. Divoky, G.S. Dutton, C. Sweeney, J.C. George, and D.U. Longenecker. 2017. Drivers and environmental responses to the changing annual snow cycle of northern Alaska. Bull. Amer. Meteor. Soc. 98(12):2559–2577. https://journals.ametsoc.org/doi/10.1175/BAMS-D-16-0201.1. doi:10.1175/BAMS-D-16-0201.1.


Learn about other indicators in this section

Wildifres  Streamflow  Stream Water Temperature  Water Temperature in the Snake River  Lake Temperature  Great Lakes Water Levels and Temperatures  Bird Wintering Ranges  The Black Guillemots of Cooper Island  Marine Species Distribution  Leaf and Bloom Dates  Cherry Blossom Bloom Dates in Washington, D.C.

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    • Tribal Connection: Trends in Stream Temperature in the Snake River
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    • A Closer Look: The Black Guillemots of Cooper Island
    • Marine Species Distribution
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    • Community Connection: Cherry Blossom Bloom Dates in Washington, D.C.
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Last updated on July 21, 2021